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Lolobau

Photo of this volcano
  • Papua New Guinea
  • Melanesia and Australia
  • Caldera
  • 1912 CE
  • Country
  • Volcanic Region
  • Primary Volcano Type
  • Last Known Eruption
  • 4.92°S
  • 151.158°E

  • 858 m
    2815 ft

  • 252130
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

The Global Volcanism Program has no activity reports for Lolobau.

The Global Volcanism Program has no Weekly Reports available for Lolobau.

The Global Volcanism Program has no Bulletin Reports available for Lolobau.

This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.

Eruptive History

There is data available for 4 Holocene eruptive periods.

Start Date Stop Date Eruption Certainty VEI Evidence Activity Area or Unit
1911 1912 Confirmed 4 Historical Observations East flank (Sili)
[ 1908 ] [ Unknown ] Uncertain    
1904 Aug 9 1905 Oct 18 (in or after) Confirmed 4 Historical Observations East flank (Sili, Malo), Hulu ?
1100 ± 30 years Unknown Confirmed 4 Radiocarbon (uncorrected) Hulu
Deformation History

There is no Deformation History data available for Lolobau.

Emission History

There is no Emissions History data available for Lolobau.

Photo Gallery

Lolobau volcano (left) is located on the western rim of a caldera that formed about 12,000 years ago on Lolobau Island. It is seen here from the south across Expectation Strait along the NE coast of New Britain. The peak at the right is on the eastern rim of the 6-km-wide caldera. Several vents within the caldera along an E-W-trending line on the E flank have had recorded activity.

Photo by Robert Citron, 1970 (courtesy of William Melson, Smithsonian Institution).
See title for photo information.
Lolobau Island lies just off the northern coast of New Britain, west of Cape Deschamp. Lolobau was constructed on the western rim of a 6-km-wide caldera. Eruptive activity from vents on the flank was observed in the early 20th century.

Photo by Robert Citron, 1970 (courtesy of William Melson, Smithsonian Institution).
See title for photo information.
Lolobau is located on the western rim of a 6-km-wide caldera, which formed about 12,000 years ago on the 8 x 13 km Lolobau Island. It is seen here from the south beyond the lower flanks of Ulawun. The smaller peak to the right is located along the eastern caldera rim.

Photo by Robert Citron, 1970 (courtesy of William Melson, Smithsonian Institution).
See title for photo information.
GVP Map Holdings

The maps shown below have been scanned from the GVP map archives and include the volcano on this page. Clicking on the small images will load the full 300 dpi map. Very small-scale maps (such as world maps) are not included. The maps database originated over 30 years ago, but was only recently updated and connected to our main database. We welcome users to tell us if they see incorrect information or other problems with the maps; please use the Contact GVP link at the bottom of the page to send us email.


Title: Sol-I Region, Topo of the
Publisher: USGS-CCOP/SOPAC S. Pacific Project
Country: Solomon Is
Year: 1983
Map Type: Bathymetric
Scale: 1:1,800,000
Map of Sol-I Region, Topo of the
Smithsonian Sample Collections Database

There are no samples for Lolobau in the Smithsonian's NMNH Department of Mineral Sciences Rock and Ore collection.

External Sites